Integration of ERT and Geotechnical Investigation for River Restoration: A Case Study of Dam Removal Site Characterization. [PDF]
Rahimi M +5 more
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Mapping potential soil erosion in East Africa using the Universal Soil Loss Equation and secondary data [PDF]
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Rain, waves, and short-term evolution of composite seacliffs in southern California [PDF]
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Are historical trends in weather consistent with model predictions in the Central United States? [PDF]
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FTIR-derived soil degradation indices and stochastic modelling of organic matter-sediment dynamics in a Mediterranean watershed: A Northern Apennines case study. [PDF]
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Spatio-temporal soil loss modelling using RUSLE and sediment delivery into a reservoir in a semi-arid region of northern Nigeria. [PDF]
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Future flood susceptibility mapping under climate and land use change. [PDF]
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Farmland hydrological cycle under agroforestry systems and efficient use of water resources in the karst desertification environment. [PDF]
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Erosive storm energy is the primary driver of soil detachment, and hence a major determinant of transfer of sediment and particulate phosphorus (P) to surface waters. Modelling of sediment and P loss at catchment scale, for example for the development of catchment and national mitigation policies, requires a spatially interpolated estimate of variation
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Abstract Rainfall kinetic energy is a widely recognized indicator of a raindrop's ability to detach soil particles in rainsplash erosion. However, it is challenging to estimate the kinetic energy (KE) of a given rain event, because it involves analysis of the terminal velocity and drop size distribution (DSD) of raindrops.
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